Jove
Visualize
Contáctanos

Videos de Conceptos Relacionados

What is Climate?01:16

What is Climate?

Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Precipitation Gravimetry01:03

Precipitation Gravimetry

Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
Precipitation Processes01:12

Precipitation Processes

The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
Microbes and Climate Change01:27

Microbes and Climate Change

Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...

También podría leer

Artículos Relacionados

Artículos vinculados a este trabajo por autores compartidos, revista y gráfico de citas.

Ordenar por
Same author

Improved latitudinal carbon budgets from global airborne surveys.

Proceedings of the National Academy of Sciences of the United States of America·2026
Same author

Disparities in stereotactic radiosurgery receipt in patients with brain metastases from non-small cell lung cancer.

Journal of neuro-oncology·2026
Same author

Middle East dust as an important external driver of the Indian Ocean Dipole.

Nature communications·2026
Same author

High Phosphate and Low Protein Mediate Arterial and Cutaneous Vascular Calcification in CKD Mice.

Journal of the American Society of Nephrology : JASN·2025
Same author

Drivers of the extreme North Atlantic marine heatwave during 2023.

Nature·2025
Same author

A lupus-derived autoantibody that binds to intracellular RNA activates cGAS-mediated tumor immunity and can deliver RNA into cells.

Science signaling·2025
Same journal

Erratum for the Research Article "Detecting supramolecular organic nanoparticles during heat wave".

Science (New York, N.Y.)·2026
Same journal

Local signals, systemic decline.

Science (New York, N.Y.)·2026
Same journal

The mechanics of liver regeneration.

Science (New York, N.Y.)·2026
Same journal

Computing in a memory with physics.

Science (New York, N.Y.)·2026
Same journal

Retraction.

Science (New York, N.Y.)·2026
Same journal

Making time.

Science (New York, N.Y.)·2026
Ver todos los artículos relacionados
JoVE
x logofacebook logolinkedin logoyoutube logo
ACERCA DE JoVE
Visión GeneralLiderazgoBlogCentro de Ayuda JoVE
AUTORES
Proceso de PublicaciónConsejo EditorialAlcance y PolíticasRevisión por ParesPreguntas FrecuentesEnviar
BIBLIOTECARIOS
TestimoniosSuscripcionesAccesoRecursosConsejo Asesor de BibliotecasPreguntas Frecuentes
INVESTIGACIÓN
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchivo
EDUCACIÓN
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualCentro de Recursos para ProfesoresSitio de Profesores
Términos y Condiciones de Uso
Política de Privacidad
Políticas

Video Experimental Relacionado

Updated: Jun 27, 2026

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites
09:05

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites

Published on: June 24, 2019

Observaciones climáticas recientes comparadas con las proyecciones.

Stefan Rahmstorf1, Anny Cazenave, John A Church

  • 1Potsdam Institute for Climate Impact Research, 14482 Potsdam, Germany.

Science (New York, N.Y.)
|February 3, 2007
PubMed
Resumen
Este resumen es generado por máquina.

Las tendencias climáticas observadas muestran un aumento del dióxido de carbono, las temperaturas globales y el nivel del mar. Datos recientes sugieren que el sistema climático, especialmente el nivel del mar, puede estar cambiando más rápido de lo que los modelos climáticos predijeron.

Más Videos Relacionados

Surface Mapping of Earth-like Exoplanets using Single Point Light Curves
06:48

Surface Mapping of Earth-like Exoplanets using Single Point Light Curves

Published on: May 10, 2020

Using Generative Art to Convey Past and Future Climate Transitions
06:10

Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

Videos de Experimentos Relacionados

Last Updated: Jun 27, 2026

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites
09:05

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites

Published on: June 24, 2019

Surface Mapping of Earth-like Exoplanets using Single Point Light Curves
06:48

Surface Mapping of Earth-like Exoplanets using Single Point Light Curves

Published on: May 10, 2020

Using Generative Art to Convey Past and Future Climate Transitions
06:10

Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

Área de la Ciencia:

  • Ciencias del clima ciencia del clima.
  • Ciencias ambientales Ciencias ambientales.
  • Ciencia del sistema de la Tierra Ciencia del sistema de la Tierra

Sus antecedentes:

  • El Informe de Evaluación de 2001 del Grupo Intergubernamental de Expertos sobre el Cambio Climático (IPCC) proporcionó proyecciones clave del modelo climático.
  • El Protocolo de Kioto, con una línea de base de 1990, estableció compromisos internacionales para la reducción de las emisiones de gases de efecto invernadero.

Objetivo del estudio:

  • Para comparar las recientes tendencias climáticas observadas con las proyecciones anteriores del modelo del IPCC.
  • Para evaluar si los cambios climáticos actuales se alinean con o exceden las predicciones anteriores.

Principales métodos:

  • Análisis de los datos observados para la concentración de dióxido de carbono, la temperatura media global del aire y el nivel global del mar desde 1990.
  • Comparación de estas tendencias observadas con las proyecciones del Informe de Evaluación del IPCC de 2001.

Principales resultados:

  • Se presentan las tendencias recientemente observadas en la concentración de dióxido de carbono, la temperatura media global del aire y el nivel global del mar.
  • La comparación indica una aceleración potencial en la respuesta del sistema climático, particularmente para el nivel del mar, en comparación con las proyecciones del modelo.

Conclusiones:

  • Los cambios climáticos observados desde 1990 plantean preocupaciones sobre la precisión de los modelos climáticos actuales.
  • El aumento del nivel del mar puede estar ocurriendo más rápidamente de lo proyectado anteriormente, lo que indica una respuesta potencialmente más rápida al cambio climático.